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西昌米市盆地砂岩型铜-铼矿床地质特征及找矿前景

唐屹 郝雪峰 彭宇 潘蒙 梁斌 陈榜巧 杨荣 范俊波 贺洋

地质通报2023,Vol.42Issue(12):2028-2036,9.
地质通报2023,Vol.42Issue(12):2028-2036,9.DOI:10.12097/j.issn.1671-2552.2023.12.002

西昌米市盆地砂岩型铜-铼矿床地质特征及找矿前景

Geological characteristics and prospecting otential of sandstone-type copper-rhenium deposits in Mishi Basin,Xichang

唐屹 1郝雪峰 1彭宇 1潘蒙 1梁斌 2陈榜巧 2杨荣 1范俊波 1贺洋1

作者信息

  • 1. 四川省地质调查院,四川 成都 610081||稀有稀土战略资源评价与利用四川省重点实验室,四川 成都 610081
  • 2. 西南科技大学环境与资源学院,四川 绵阳 621000
  • 折叠

摘要

Abstract

A new rhenium ore body associated with sandstone-type copper deposits was discovered in the Lower Cretaceous Feitianshan Formation(K1f)of the Mishi Mesozoic continental basin in Zhaojue-Puge,Xichang.This article mainly introduces the distribution of the copper-rhenium deposit(occunence)and the characteristics of the ore body,and preliminary analysis of the genesis and prospecting potential of the ore deposit.The discovered deposits(occurrences)are layered and lenticular distributed in sandstone.The main ore types are fragmented and lenticular sandstones with bituminous bands.The ores of the deposit have relatiively high Cu,Re and Ag,with the content of Cu 0.23%~39.10%,average 7.23%;Re content 2.76~131.49 g/t,average 24.70 g/t,Ag content 41.4~384 g/t,which can be called Cu-Re-Ag sandstone deposit.The mineralization is closely related to organic matter such as bitumen.It is preliminarily believed that the mineralization of rhenium and other elements is closely related to the formation and evolution of ancient oil reservoirs.The Feitianshan Formation(KJ)ore-bearing horizon in the Mishi Basin is relatively stable,with obvious prospecting signs and great prospecting potential.

关键词

铼矿/稀散金属/有机质/西昌/找矿前景

Key words

rhenium deposit/dispersed element/organic matter/Xichang/prospecting potential

分类

天文与地球科学

引用本文复制引用

唐屹,郝雪峰,彭宇,潘蒙,梁斌,陈榜巧,杨荣,范俊波,贺洋..西昌米市盆地砂岩型铜-铼矿床地质特征及找矿前景[J].地质通报,2023,42(12):2028-2036,9.

基金项目

四川省自然资源厅2020年省政府性投资地质勘查(第一批)项目《四川盆地及周边中生代陆相沉积建造中钼、铼等稀有稀散元素资源富集规律基础调查》(编号:DZ202006) (第一批)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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